2016 Publication Year 2020-04-30T16:04:26Z Acceptance

Total Page:16

File Type:pdf, Size:1020Kb

2016 Publication Year 2020-04-30T16:04:26Z Acceptance Publication Year 2016 Acceptance in OA@INAF 2020-04-30T16:04:26Z Title PRISMA, Italian network for meteors and atmospheric studies Authors GARDIOL, Daniele; CELLINO, Alberto; DI MARTINO, Mario Handle http://hdl.handle.net/20.500.12386/24394 76 Proceedings of the IMC, Egmond, 2016 PRISMA Italian network for meteors and atmospheric studies Daniele Gardiol, Alberto Cellino and Mario Di Martino INAF ± Osservatorio Astrofisico di Torino, Pino Torinese, Italia [email protected] The aim of the PRISMA project is to develop the Italian participation in a network of European observing facilities whose primary targets are bright meteors (the so-called bolides and fireballs) and the recovery of meteorites. Several all-sky cameras have been recently installed in France (FRIPON project), and we propose to do the same in Italy, interconnecting the Italian network with the French one. Such a network is of great interest for the studies of interplanetary bodies and the dynamical and physical evolution of the population of small bodies of the Solar System and for the studies of collected meteorites. Those eventually recovered will be classified and investigated from the petrologic, genetic and evolutionary points of view, analyzed for their spectral characteristics and compared with known asteroids. The possibility to measure the radioactivity of samples shortly after the fall using gamma-ray spectrometers available in the Osservatorio Astrofisico di Torino laboratories, will allow us to reveal the presence of short-lived cosmogenic radioisotopes. PRISMA is also very suitable for the purposes of atmospheric studies. This includes the statistics of cloud coverage and lightning frequencies, as well as the comparison of the optical depth measured using satellites and PRISMA cameras. 1 Scientific motivations been exposed to terrestrial alteration, which makes them scientifically less valuable. A way to reliably determining PRISMA for meteor studies the source regions of meteorites is to witness the falls Meteorites represent samples of Solar System bodies when they occur. For this purpose, the same event should naturally brought to our labs from a variety of different be detected simultaneously from different directions, in locations. Dynamical studies suggest that most meteorites order to be able to derive at the same time the original come from the asteroid main belt, rather than from the heliocentric orbit of the impactor and the site of fall of closer population of so-called near-Earth asteroids, as possible meteorites produced by the event. This has been commonly believed (Burbine, 2002). However, it is the goal inspiring many observation networks, such as the difficult to conclusively identifying possible links European Fireball Network in middle-Europe, the NASA between some individual asteroids and some meteorite All-sky Fireball Network1 in the USA, and a similar one classes. It is therefore important to develop ground-based in Australia2. In this context a new generation of observations of meteor phenomena to improve our detectors optimized for the studies of bright meteors and capability of deriving accurate orbits of the small bodies the establishment of a much wider network of automatic impacting our planet, to monitor a statistically sufficient observing stations, with a grid spacing of 60±100 km, number of events to study their origin and possibly to operating 24 hours per day, can allow us to obtain a UHFRYHU³IUHVK´PHWHRULWHV. The currently open scientific major improvement. The French community (Colas, problems for which we can expect to get some important 2012; Colas 2014) has recently accomplished the first answers from an extensive work of detection of fireballs steps forward to start this enterprise (FRIPON, Fireball and recovery of freshly fallen meteorites include the Recovery and Inter Planetary matter Observation following questions: Network)3. Doing the same in Italy would give a decisive contribution to a full European network. x Where do meteorites come from? x How many parent bodies of known meteorites can PRISMA for atmospheric studies we surely identify? The inherently multi-disciplinary nature of the project x Can we better understand the mechanisms of makes it appealing to a wide scientific community. In the delivery from the asteroid main belt? field of atmospheric science, cloudiness forecasting is a x What is the abundance of water possibly delivered to challenge for numerical models. To validate current the Earth by different classes of asteroids? numerical models of cloud cover it is essential to x Are there new classes of meteorites that we have not compare simulations with large amounts of yet discovered? measurements. Data detected by all-sky cameras are useful for this and other branches of atmospheric physics The latter question is not academic. Actually, many (Arbizu-Barrena, 2015). In this respect PRISMA is PHWHRULWHV SUHVHQWO\ LQ RXU FROOHFWLRQV DUH ³ILQGV´ DV RSSRVHG WR ³IDOOV´ i.e. meteorites found a significant 1 http://fireballs.ndc.nasa.gov amount of time after their fall, often weathered having 2 http://fireballsinthesky.com.au 3 http://www.fripon.org Proceedings of the IMC, Egmond, 2016 77 complementary to traditional weather ground networks, transmitted to the data processing center where they are such as the ones operated by Agenzia Regionale Per saved and stored. O¶Ambiente (ARPA), Local Governments and other Institutions. The continuous sky monitoring by PRISMA Table 1 ± Meteorite falls and finds on Italian soil. can provide much additional information on the status of Name Region Year the atmosphere, including also statistics of lightning. Albareto Emilia-Romagna 1766 Fall )LQDOO\WKHVN\¶VSRODUL]DWLRQLVVHQVLWLYHWRWKHDHURVRO Alessandria Piemonte 1860 Fall properties in the sky and it is an ideal complementary measurement device in combination with aerosol optical Alfianello Lombardia 1883 Fall depth measurements. Assisi Umbria 1886 Fall Bagnone Toscana 1904 Find Barbianello Lombardia 1960 Find Barcis Friuli V.G. 1950 Find Borgo S.Donino Emilia-Romagna 1808 Fall Castel Berardenga Toscana 1791 Fall Castenaso Emilia-Romagna 2003 Find Castiglione d. Lago Umbria 1970 Find Castrovillari Calabria 1583 Fall Cereseto Piemonte 1840 Fall Collescipoli Umbria 1890 Fall Fermo Marche 1996 Fall Girgenti Sicilia 1853 Fall Lago Valscura Piemonte 1995 Find Masua Sardegna 1967 Find Messina Sicilia 1955 Fall Mineo Sicilia 1826 Fall Figure 1 ± Meteorite falls and finds on italian soil since Monte Milone Marche 1846 Fall the beginning of times. Motta dei Conti Piemonte 1868 Fall Narni Umbria 921 Fall 2 Project description Noventa Vicentina Veneto 1971 Fall Orvinio Lazio 1872 Fall Project description The project consists of the installation of a network of Patti Sicilia 1922 Fall fireball detectors. We plan to use the same typology of Piancaldoli Toscana 1968 Fall detectors adopted in France in the framework of the Renazzo Emilia-Romagna 1824 Fall FRIPON project, which started operations in early 2016. 5LYROWDGH¶%DVVL Lombardia 1491 Fall These detectors are cutting edge technology. The goal of San Michele Marche 2002 Fall PRISMA is to develop a full Italian network, suitably covering the national territory. The planned camera grid Siena Toscana 1794 Fall distribution will make it possible to derive the orbital Sinnai Sardegna 1956 Fall paths of the impactors with an accuracy of the order of Tessera Veneto 2000 Fall 200 meters. The first nodes of the grid will be hosted in Torino Piemonte 1988 Fall North-Western Italy, to be easily interconnected with the FRIPON network. The fireball detectors have a 100% Trenzano Lombardia 1856 Fall duty cycle, as bright fireballs can be detected even in Vago Veneto 1668 Fall daytime. The cameras operate at the wavelengths of Valdinizza Lombardia 1903 Fall visible light, with an estimated visual magnitude limit as Valdinoce Emilia-Romagna 1496 Fall faint as m = 2-3. Each camera is connected to the v Vigarano Emilia-Romagna 1910 Fall internet, and will acquire data at a maximum frequency of 30 frames per second, with recording starting in case of Expected rates detection of a bright moving source, according to Over Italy we can expect to have about 1 bright meteor triggering conditions defined by the automatic software every 48 hours. Among these events, according to current of data processing. Every 10 minutes the camera takes a estimates (Halliday, 1996), we can expect, in a country as longer single exposure for astrometric calibration and extended as Italy, the recovery rate of meteorites to be other purposes, including public outreach and further somewhere between 2 and 10 per year, these numbers scientific processing, such as for atmosphere studies. depending critically on whether the corresponding Detections and long exposures are automatically 78 Proceedings of the IMC, Egmond, 2016 fireball is seen or not. The actual recovery fraction has in particular Università di Torino, Università di Firenze been very low in the past (see Table 1 for a complete list and Università di Padova, and with the Consiglio of confirmed Italian meteorites, including the very recent Nazionale delle Ricerche (CNR)8. We are developing our confirmation of Castiglione del Lago, and Figure 1 for a outreach activities in contact with Infini.to (Museum of geographical distribution), only less than 40 meteorites Astronomy and Space ± Planetarium of Torino)9 and with have been recovered (and among them only 32 are falls) Museo Regionale di Scienze Naturali10 and Museo since the beginning of times.
Recommended publications
  • The M~Neralogical Composition and Structure of the Assisi Meteorite
    595 The m~neralogical composition and structure of the Assisi meteorite By G. R. LEvI-DoNATI (Doctor in Natural Sciences) Istituto di Mineralogia, Facolth di Scienze, Universit~ di Perugia, Italy [Taken as read 2 November 1966] Summary. The principal data about the fall and the distribution of the fragments of the Assisi (Perugia, Italy) meteorite are collected. A fragment of the stone, weighing 146.5 g, preserved in the British Museum (Natural History) (B.M. 63621), is described in some detail. Crust morphology, mineralogical composition, and structure are studied. Optical data are established by microscopical analysis of five thin sections and two polished surfaces. Compared with electron-probe analysis, they are found in good agreement. Assisi is an olivine-bronzite chondrite, H group, with characteristic features of metamorphism. N 24 May 1886, at 7 a.m., the sky being clear, a single stone weigh- O ing 1795 g fell in a cornfield in Tordandrea, 7"5 Km south-west of Assisi (Perugia, Italy). Three peasants were present and immediately unearthed the small meteorite. It was at a depth of about 60 cm, in an apparently vertical hole about 25 cm in diameter. The stone was 13.8 cm long, 12.8 cm wide. The fall was first described by Bellucci (1887), who submitted the individual specimen to a macroscopic examination. In the same year the complete meteorite was sent by Be]lucci to Vienna, where Eger made a cast of the stone and sawed the meteorite in several pieces. 1 Museums and collections later purchased the fragments, which (1967) are now widely distributed (B.
    [Show full text]
  • Japan Geoscience Union Meeting 2009 Presentation List
    Japan Geoscience Union Meeting 2009 Presentation List A002: (Advances in Earth & Planetary Science) oral 201A 5/17, 9:45–10:20, *A002-001, Science of small bodies opened by Hayabusa Akira Fujiwara 5/17, 10:20–10:55, *A002-002, What has the lunar explorer ''Kaguya'' seen ? Junichi Haruyama 5/17, 10:55–11:30, *A002-003, Planetary Explorations of Japan: Past, current, and future Takehiko Satoh A003: (Geoscience Education and Outreach) oral 301A 5/17, 9:00–9:02, Introductory talk -outreach activity for primary school students 5/17, 9:02–9:14, A003-001, Learning of geological formation for pupils by Geological Museum: Part (3) Explanation of geological formation Shiro Tamanyu, Rie Morijiri, Yuki Sawada 5/17, 9:14-9:26, A003-002 YUREO: an analog experiment equipment for earthquake induced landslide Youhei Suzuki, Shintaro Hayashi, Shuichi Sasaki 5/17, 9:26-9:38, A003-003 Learning of 'geological formation' for elementary schoolchildren by the Geological Museum, AIST: Overview and Drawing worksheets Rie Morijiri, Yuki Sawada, Shiro Tamanyu 5/17, 9:38-9:50, A003-004 Collaborative educational activities with schools in the Geological Museum and Geological Survey of Japan Yuki Sawada, Rie Morijiri, Shiro Tamanyu, other 5/17, 9:50-10:02, A003-005 What did the Schoolchildren's Summer Course in Seismology and Volcanology left 400 participants something? Kazuyuki Nakagawa 5/17, 10:02-10:14, A003-006 The seacret of Kyoto : The 9th Schoolchildren's Summer Course inSeismology and Volcanology Akiko Sato, Akira Sangawa, Kazuyuki Nakagawa Working group for
    [Show full text]
  • A Magnetic Susceptibility Database for Stony Meteorites
    Direttore Enzo Boschi Comitato di Redazione Cesidio Bianchi Tecnologia Geofisica Rodolfo Console Sismologia Giorgiana De Franceschi Relazioni Sole-Terra Leonardo Sagnotti Geomagnetismo Giancarlo Scalera Geodinamica Ufficio Editoriale Francesca Di Stefano Istituto Nazionale di Geofisica e Vulcanologia Via di Vigna Murata, 605 00143 Roma Tel. (06) 51860468 Telefax: (06) 51860507 e-mail: [email protected] A MAGNETIC SUSCEPTIBILITY DATABASE FOR STONY METEORITES Pierre Rochette1, Leonardo Sagnotti1, Guy Consolmagno2, Luigi Folco3, Adriana Maras4, Flora Panzarino4, Lauri Pesonen5, Romano Serra6 and Mauri Terho5 1Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy [[email protected]] 2Specola Vaticana, Castel Gandolfo, Italy 3Antarctic [PNRA] Museum of Siena, Siena, Italy 4Università La Sapienza, Roma, Italy 5University of Helsinki, Finland 6“Giorgio Abetti” Museum of San Giovanni in Persiceto, Italy Pierre Rochette et alii: A Magnetic Susceptibility Database for Stony Meteorites 1. Introduction the Museo Nationale dell’Antartide in Siena [Folco and Rastelli, 2000], the University of More than 22,000 different meteorites Roma “la Sapienza” [Cavaretta Maras, 1975], have been catalogued in collections around the the “Giorgio Abetti” Museum in San Giovanni world (as of 1999) of which 95% are stony types Persiceto [Levi-Donati, 1996] and the private [Grady, 2000]. About a thousand new meteorites collection of Matteo Chinelatto. In particular, are added every year, primarily from Antarctic the Antarctic Museum in Siena is the curatorial and hot-desert areas. Thus there is a need for centre for the Antarctic meteorite collection rapid systematic and non-destructive means to (mostly from Frontier Mountain) recovered by characterise this unique sampling of the solar the Italian Programma Nazionale di Ricerche in system materials.
    [Show full text]
  • Report of the United States National Museum
    — THE METEORITE COLLECTION IN THE U. S. NATIONAL MUSEUM; A CATALOGUE OF METEORITES REPRESENTED NOVEMBER 1, 1886, By F. W. Clarke. The following catalogue has been prepared mainly to facilitate ex- changes and to aid in the upbuilding of the collection. In addition to the usual information as to title, date of fall, and weight of specimen, it has beeu thought well to give the source from which each example was obtained ; and it may be interesting to note that the meteorites ac- credited to Dr. J. Berrien. Lindsley were mainly received by him from the late Dr. J. Lawrence Smith. In the catalogue of the Shepard col- lection, now on deposit in the Museum, the arrangement of Professor Shepard himself has been followed without change. Including the Shepard meteorites, over 200 falls are now on exhibition, giving the entire collection a very respectable place among the larger collections of the world. The Tucson iron is unique, and therefore a cut of it is inserted. METEORIC IRONS. 1. Scriba, Oswego County, N. Y. Fouud about 1834. Fragment, 9.15 grammes. By exchange from S. C. H. Bailey. 2. Burlington, Otsego County, N. Y. Ploughed up previous to 1819. Weight of specimen, 76.87 grammes. By exchange from Prof. C. U. Shepard. 3. Lockport, Niagara County, N. Y. Ploughed up earlier thau 1845. Slice weigh- ing 155 grammes. By exchange from the cabinet of Yale College. 4. Jenny's Cheek, Wayne County, W. Va. Found in 1884. Several small frag- ments, 25.5 grammes in all; largest fragment, 15.3 grammes.
    [Show full text]
  • The Meteorite Collection in the Natural Science Museum of Turin1
    CSIRO PUBLISHING www.publish.csiro.au/journals/pasa Publications of the Astronomical Society of Australia, 2009, 26, 259–265 The Meteorite Collection in the Natural Science Museum of Turin1 E. CostaA,C and L. M. GalloB A Dipartimento di Scienze Mineralogiche e Petrografiche, Università degli Studi di Torino – Via Valperga Caluso 35, I–10136 Torino, Italy B Museo Regionale di Scienze Naturali, Sezione di Mineralogia, Petrografia e Geologia – Via G. Giolitti 36, I–10123 Torino, Italy C Corresponding author. Email: [email protected] Received 2008 November 11, accepted 2009 February 16 Abstract: The Natural Science Museum of Turin is the owner of a small but nice collection of meteorites, partly obtained by means of direct acquisition during the last 30 years, and partly inherited from the rather old collection of the University of Turin. This collection was partially forgotten for the last 50 years, and after 1936 the collection became almost invisible. In the last 30 years the meteorite samples were tightly packaged and retained in the basement of the museum building. Currently a new listing of the meteorite collection is in progress and almost finished, in which every sample is described, measured and weighed. For each sample the authors acquired high resolution images and examined historical documentations. Images were acquired with a desktop scanner, which was found to be an ideal tool for this purpose. A classification based on most famous meteorite catalogues is coupled to each description. About eighty samples (and probably a new meteorite, not described until now) will be depicted in the new catalogue, which hopefully will be published during 2009.
    [Show full text]
  • Oral Hist Honda.Fm
    Meteoritics & Planetary Science 38, Nr 7, Supplement, A177–A187 (2003) Abstract available online at http://meteoritics.org Report Oral histories in meteoritics and planetary science: XI. Masatake Honda Ursula B. MARVIN Harvard-Smithsonian Center for Astrophysics, Cambridge, Massachusetts 02138, USA E-mail: [email protected] (Received 27 May 2003) Abstract–Masatake Honda majored in inorganic chemistry at the University of Tokyo and then pursued graduate studies in geochemistry. In 1943, he completed his first research project, which yielded new data on the behavior of strontium in carbonates. He then spent the next two years as a technical officer in the Japanese Imperial Navy. While on duty, he gained expertise in the important new field of ion exchange methods, which he ultimately chose as the topic for his Ph.D. thesis and then expanded into a book. In 1955, Honda traveled to Switzerland and spent a year in research laboratories at Bern and Zürich. He then joined Professor James R. Arnold at Princeton University and soon began focusing his research on cosmic-ray produced nuclides in meteorites. Two years later, he accompanied Dr. Arnold to the University of California at La Jolla where they joined the research group of Professor Harold C. Urey. Honda developed techniques for measuring terrestrial ages of meteorites and showed that most of them have survived weathering for vastly longer periods than had been anticipated. After spending nearly eight years abroad, he returned to Japan in 1962 as a full professor at the University of Tokyo. During the Apollo missions, he performed research on cosmogenic nuclides in lunar rocks, surface soils, and deep drill cores.
    [Show full text]
  • Petrogenesis of Main Group Pallasite Meteorites Based on Relationships
    Vrije Universiteit Brussel Petrogenesis of main group pallasite meteorites based on relationships among texture, mineralogy, and geochemistry Mckibbin, Seann; Pittarello, Lidia; Makarona, Christina; Hamman, Christopher; Hecht, Lutz; Chernonozhkin, Stepan; Goderis, Steven; Claeys, Philippe Published in: Meteoritics & Planetary Science DOI: 10.1111/maps.13392 Publication date: 2019 Link to publication Citation for published version (APA): Mckibbin, S., Pittarello, L., Makarona, C., Hamman, C., Hecht, L., Chernonozhkin, S., ... Claeys, P. (2019). Petrogenesis of main group pallasite meteorites based on relationships among texture, mineralogy, and geochemistry. Meteoritics & Planetary Science, 54(11), 2814-2844. https://doi.org/10.1111/maps.13392 General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Download date: 03. Oct. 2021 Meteoritics & Planetary Science 1–31 (2019) doi: 10.1111/maps.13392 Petrogenesis of main group pallasite meteorites based on relationships among texture, mineralogy, and geochemistry 1,5,6* 1,7 1 Seann J.
    [Show full text]
  • CASTENASO'' Una Nuova Meteoriteitaliana
    Quoderno di Srudi e Notizie di Storio Nqfurqle dello Romogno Quad.Studi Nal Romagn422:129-135, giugno 2006 ISSN1123-67s7 Notizie Naturalistiche FrancoMeriehi CONDRITE ORDINARIA''CASTENASO'' Una nuova meteoriteitaliana Nonostante io sia molto interessato alla conoscenza delle meraviglie della Natura e partecipi alle tante iniziative che si adoperanoper la salvaguardiadel nostro pianeta e di tutto ciò che vive in esso, mi sono reso conto che, come la grande maggioranza delle persone, ho una conoscenzaassolutamente insuffr- cientedel firmamento,dei misteri e degli equilibri dell'Universo. Sonocerto che una migliore conoscenzadi questi misteri e di questi equilibri potrebbe indurre l'Uomo ad esserepiù consapevoledella propria fragilità e più rispettosoverso la "martoriata" madre Terra, che ci manda segnali che fingiamo di non capire e ci awerte a modo suo dei tanti equilibri che si stanno rompendo. Per soddisfarele mie curiosità e migliorare le mie scarseconoscenze, qualche anno fa partecipai ad un corso di astronomiadella durata di una ventina di giorni. Quella esperienzami ha cambiato la vita, mi ha fatto capire quanto io, essere "arrogante umano e presuntuoso", fossi niente di fronte all'immensità dell'Universo.Fra l'altro, mi ha molto colpito apprendereche esistenel sistema solare, tra Marte e Giove, la fascia degli Asteroidi, composta da miliardi di pianetini (gli Asteroidi), grandi e piccoli frammenti di roccia e metallo, rimasti a vagareorbitando intomo al Sole, dai tempi della formazione del sistemasolare. Come tutti i pianeti, si sono formati, nello stessotempo e con la stessamateria, insieme al Sole, che pure stava nascendocirca quattro miliardi e mezzo di anni fa. Alcuni di questi frammenti collidendo tra loro o per altre causenon sempre accertate,escono dalla fascia degli Asteroidi ed intersecanole orbite dei pianeti intemi, venendo catturati dalla loro forzadi gravità.
    [Show full text]
  • Annual Report of the Board of Regents of the Smithsonian Institution
    SECTIOlSr I. REP () K T VrON THK CONDITION AND PROGRESS OF THE U. S. NATIONAL MUSEUM DURING THE YEAR ENDING JUNE 30, 1891. G. BROWN GOODE, ASSISTANT SKCKETARY OF THK SMITHSONIAN INSTITUTION, IN CHARGE OF V. S. NATIONAL MUSEUM. SM 91, PT 2 1 KEPORT UPON S. NATIONAL MUSEUM THF CONDITION AND PROGRESS OF THE U. DURING THE YEAR ENDING JUNE BO, 1891. BY G. Brown Goode, Museum, Institution, in charge of U. S. National Assistant Secretan,, Smmsonian A.—GENERAL CONSIDEEATIONS. statement of the operations of the Before, entering upon a detailed Report, it is perhaps not Musenni during the period covered by tliis organization, and aims, in order undesirable to briefly outline its history, work now to be reported upon, as the that the true relationships of the be comprehended. outoTowth of the activities of other years, may by act of Congress m The Smithsonian Institution was established that '' all objects of art and 184G One of the provisions of the act was and all objects of natural history, of foreign and curious research, mineralogical specimens " belonging to the plants, and geological and of the Institution, to be ar- United States should be placed in the custody students. It was also pro- r-m-ed and classified so as to be available for of objects known as - the National ^dded that a miscellaneous collection accumulated in the Patent Oftice, Cabinet of Curiosities," which had beginning was thus made should be transferred to the Institution.* A which, however, was not recognized othcially for the National Museum, The various steps which under that designation until a later date.
    [Show full text]
  • The Orbits of Meteorites from Natural Thermoluminescence
    NASMCR---- _7 _7-- 207733 ./:;;/:y :',v" • ii., (:- _ -_"Z_- Attachment 5 ICAm:S 125. 281-287 (1997) \RTICLE Nf). IS965622 : i .'i_.-' /..¢__.,_"_7. _,, _1, j The Orbits of Meteorites from Natural Thermoluminescence P. H. BENOIT AND D. W. G. SEARS Cosmochemistry (Troup, Department of Chemistry and Biochemistry. University of Arkansas. Fayetteville. Arkansas 72701 E-mail: [email protected] Received December 15, 1995; revised July 29, 1996 The possible existence of meteoroid streams, even as The natural thermoluminescence (TL) of meteorites reflects relatively minor contributors to the terrestrial flux of extra- their irradiation and thermal histories. Virtually all ordinary terrestrial material, is important in understanding the or- chondrites have been irradiated long enough to have reach bital evolution of meteoroid bodies, the rarity of potential saturation natural TL levels, and thus natural TL levels in asteroidal sources for ordinary chondrites, which account these meteorites are determined largely by thermal history. The for more than 60% of meteorite falls (Greenberg and Nolan primary heat source for most meteorites is the Sun, and thus 1989), and apparent differences between meteorites cur- natural TL levels are determined primarily by the closest ap- rently falling and those that fell over the last few hundred proach to the Sun, i.e., perihelion. By converting natural TL thousand years and have been stored in the ice sheet of levels to perihelia, using an assumed albedo typical of meteoroid Antarctica (Koeberl and Cassidy 1991, Benoit and Sears bodies, it is found that most ordinary chondrites had perihelia of 0.85 to 1.0 AU prior to reaching Earth.
    [Show full text]
  • Radial Distribution of Spallogenic K, Ca, Ti, V and Mn Isotopes in Iron Meteorites Mineo Imamura *, Masako Shima **, and Masatake Honda
    Radial Distribution of Spallogenic K, Ca, Ti, V and Mn Isotopes in Iron Meteorites Mineo Imamura *, Masako Shima **, and Masatake Honda The Institute for Solid State Physics, The University of Tokyo Z. Naturforsch. 35 a, 267-279 (1980); received January 7, 1980 Dedicated to Professor H. Hintenberger on the occasion of his 70tli birthday Cosmic-ray-produced stable nuclides of Ca (mass number: 42, 43, 44 and 46), Ti (46, 47, 49 and 50), V (50), Cr (50, 53 and 54) and the long-lived nuclides, 40K and 53Mn were determined along the radial axes of the iron meteorites Grant and Treysa. Grant was extensively examined and the results compared with rare gas data. Although Treysa does not include enough samples to allow detailed analysis, the depth profile shows typical features for a small meteorite. The results were compared with calculated profiles of 40K, 49Ti and 53Mn using thick bombard- ment data. The approximate pre-atmospheric radii of Grant and Treysa were determined to be 30 cm and 14 cm, respectively. The effect of space erosion was also estimated by comparing the data of 49Ti and radioactive 53Mn in Grant and Treysa with the calculated patterns. It is suggested that space erosion of both meteorites is small (<0.8Ä/y) during the cosmic-ray exposure of several hundred million years. 1. Introduction Among the spallogenic nuclides in iron meteorites, the production rate of rare-gas isotopes decreases The interaction of primary cosmic radiation with with the depth of the sample, that is, production cor- meteorites produces many secondary particles of relates almost linearly with the attenuation of high various energies, causing very complex nuclear energy particles.
    [Show full text]
  • Xb Ie'ian%Mlseltm
    Xb1oxfitateie'ian%Mlseltm PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK 24, N.Y. NUMBER 2 I 90 SEPTEMBER IO, I964 The Meteorite and Tektite Collection of the American Museum of Natural History BY BRIAN MASON' INTRODUCTION The first meteorite received by the American Museum of Natural History was a 46-gram piece of the Searsmont chondrite, presented by G. M. Brainerd of Rockland, Maine, in 1872. For some years the col- lection grew very slowly. Hovey (1896) published the first catalogue, in which he enumerated 55 pieces representing 26 different meteorites. However, the status of the collection was radically changed in 1900 with the acquisition of the Bement collection of minerals, through the gener- osity ofJ. Pierpont Morgan. Besides some 12,000 mineral specimens, the Bement collection contained 580 meteorites, representing nearly 500 different falls and finds. This acquisition established the meteorite col- lection of this museum as one of the great collections of the world, a situation that has been maintained by more recent additions. Some of the more notable additions may be briefly noted. In 1904 three Cape York irons, brought from Greenland in 1897 by R. E. Peary, were deposited in the museum. These are known as "Ahnighito" or "The Tent," "The Woman," and "The Dog" (fig. 1). "Ahnighito," the largest of the three, is approximately 11 feet long, 7 feet high, and 6 feet thick. Various estimates of its weight, ranging from 30 to 80 tons, have been published. Thanks to the Toledo Scale Company it was mounted 1 Chairman, Department of Mineralogy, the American Museum of Natural History.
    [Show full text]